Dynamics of the Makassar Strait
Data collected as part of the Arlindo Project ("Arlindo" is an acronym for Arus Lintas Indonesia, meaning "throughflow" in Bahasa Indonesia) from October 1996 to March 1998 are analyzed to study the characteristics of the flow through the Makassar Strait. Analysis of inverted ech...
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| Veröffentlicht in: | Journal of marine research 2001-03, Vol.59 (2), p.313-325 |
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| container_title | Journal of marine research |
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| creator | Waworuntu Garzoli, Silvia L. Olson, Donald B. |
| description | Data collected as part of the Arlindo Project ("Arlindo" is an acronym for Arus Lintas Indonesia, meaning "throughflow" in Bahasa Indonesia) from October 1996 to March 1998 are analyzed to study the characteristics
of the flow through the Makassar Strait. Analysis of inverted echo sounders (IES) and bottom pressure data (PIES) combined with TOPEX/POSEIDON satellite-derived sea height anomaly suggest that a minimum
of three-layer approximation is necessary to explain the dynamics of the flow in the Makassar Strait. The simple two-layer model used in several studies of the throughflow is rejected based on total incompatibility
with the data sets. A three-layer model with significant contributions by the middle layer provides a consistent interpretation of PIES and satellite data. Results are interpreted in the framework of the
large-scale circulation. |
| doi_str_mv | 10.1357/002224001762882673 |
| format | Article |
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of the flow through the Makassar Strait. Analysis of inverted echo sounders (IES) and bottom pressure data (PIES) combined with TOPEX/POSEIDON satellite-derived sea height anomaly suggest that a minimum
of three-layer approximation is necessary to explain the dynamics of the flow in the Makassar Strait. The simple two-layer model used in several studies of the throughflow is rejected based on total incompatibility
with the data sets. A three-layer model with significant contributions by the middle layer provides a consistent interpretation of PIES and satellite data. Results are interpreted in the framework of the
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of the flow through the Makassar Strait. Analysis of inverted echo sounders (IES) and bottom pressure data (PIES) combined with TOPEX/POSEIDON satellite-derived sea height anomaly suggest that a minimum
of three-layer approximation is necessary to explain the dynamics of the flow in the Makassar Strait. The simple two-layer model used in several studies of the throughflow is rejected based on total incompatibility
with the data sets. A three-layer model with significant contributions by the middle layer provides a consistent interpretation of PIES and satellite data. Results are interpreted in the framework of the
large-scale circulation.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Marine</subject><subject>Ocean currents</subject><subject>Oceanography</subject><subject>Physics of the oceans</subject><subject>Thermohaline structure and circulation. Turbulence and diffusion</subject><issn>0022-2402</issn><issn>1543-9542</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNp1kN9rFDEQgINU8Fr9B3zxkOLbambyc59KuWortPigPoe5bPa6173dNskJ9a83e3dgqRgImYRvvpkMY2-BfwShzCfOEVFyDkajtaiNeMFmoKSoaiXxiM0moCoEvmLHKa3LVUttZuzdxeNAm86n-djO822Y39AdpURx_j1H6vJr9rKlPoU3h_OE_fzy-cfiqrr-dvl1cX5dealsrppWGPC88RyNFWB9Iz2BsprCsrwvZaOUrS0Bab-suREGKXgftBQQeGjFCfuw997H8WEbUnabLvnQ9zSEcZscWG6B17aA75-B63Ebh9KbQ4DagFFYINxDPo4pxdC6-9htKD464G4amPt3YCXp9GCm5KlvIw2-S08yNZc4uc_2WDeswpDpb_31Ju42Fm0pMC1VHwKOjmKeAl0MN_8xdH4nODSH7peqByw-LF9HdKBAuSa0tO2zyxTd6rdLWvwBnh-U4g</recordid><startdate>20010301</startdate><enddate>20010301</enddate><creator>Waworuntu</creator><creator>Garzoli, Silvia L.</creator><creator>Olson, Donald B.</creator><general>Sears Foundation for Marine Research</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>SOI</scope></search><sort><creationdate>20010301</creationdate><title>Dynamics of the Makassar Strait</title><author>Waworuntu ; Garzoli, Silvia L. ; Olson, Donald B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c458t-df371c0dc0278318cd4ca1586aeb1c0b4d55898a1a6cb907372aecce6431e0ef3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2001</creationdate><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Marine</topic><topic>Ocean currents</topic><topic>Oceanography</topic><topic>Physics of the oceans</topic><topic>Thermohaline structure and circulation. Turbulence and diffusion</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Waworuntu</creatorcontrib><creatorcontrib>Garzoli, Silvia L.</creatorcontrib><creatorcontrib>Olson, Donald B.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Environment Abstracts</collection><jtitle>Journal of marine research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Waworuntu</au><au>Garzoli, Silvia L.</au><au>Olson, Donald B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Dynamics of the Makassar Strait</atitle><jtitle>Journal of marine research</jtitle><date>2001-03-01</date><risdate>2001</risdate><volume>59</volume><issue>2</issue><spage>313</spage><epage>325</epage><pages>313-325</pages><issn>0022-2402</issn><eissn>1543-9542</eissn><coden>JMMRAO</coden><abstract>Data collected as part of the Arlindo Project ("Arlindo" is an acronym for Arus Lintas Indonesia, meaning "throughflow" in Bahasa Indonesia) from October 1996 to March 1998 are analyzed to study the characteristics
of the flow through the Makassar Strait. Analysis of inverted echo sounders (IES) and bottom pressure data (PIES) combined with TOPEX/POSEIDON satellite-derived sea height anomaly suggest that a minimum
of three-layer approximation is necessary to explain the dynamics of the flow in the Makassar Strait. The simple two-layer model used in several studies of the throughflow is rejected based on total incompatibility
with the data sets. A three-layer model with significant contributions by the middle layer provides a consistent interpretation of PIES and satellite data. Results are interpreted in the framework of the
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| ispartof | Journal of marine research, 2001-03, Vol.59 (2), p.313-325 |
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| language | eng |
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| source | EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
| subjects | Earth, ocean, space Exact sciences and technology External geophysics Marine Ocean currents Oceanography Physics of the oceans Thermohaline structure and circulation. Turbulence and diffusion |
| title | Dynamics of the Makassar Strait |
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